CAJ | 학술논문

刘戈庄石墨矿为赋存于古元古代荆山群陡崖组徐村段含石墨变质岩系地层中的沉积变质型矿床,严格受地层层位控制,含矿岩性为石墨黑云斜长片麻岩、石墨透辉变粒岩、石墨透闪透灰岩,变质相达麻粒岩相,经历多期区域变质作用形成。该文采用最新成矿理论,对典型矿床的构造背景、物质来源进行了研究,确定了刘戈庄石墨矿矿床成矿模式,对利用该模式进行石墨矿成矿预具有一定的指导意义。
류과장석묵광위부존우고원고대형산군두애조서촌단함석묵변질암계지층중적침적변질형광상,엄격수지층층위공제,함광암성위석묵흑운사장편마암、석묵투휘변립암、석묵투섬투회암,변질상체마립암상,경력다기구역변질작용형성。해문채용최신성광이론,대전형광상적구조배경、물질래원진행료연구,학정료류과장석묵광광상성광모식,대이용해모식진행석묵광성광예구유일정적지도의의。
Systematic graphite deposit prospecting work in Shandong province began in 1957.It mainly concentrated in Nanshu area of Laixi city,and submitted a large number of exploration achievements.Nanshu graphite deposit is a sedimentary metamorphic deposit in grahpite-bearing metamorphic rocks in Xucun setion of Douya formation in Proterozoic Jingshan group.It is strictly controlled by stratigraphic strata,and experienced multi-phase regional metamorphisms.Shandong graphite deposits have the same origin with Nanshu graphite deposit.Thus,such graphite deposits in Shandong province are named as ＂Nanshu type＂ graphite deposits in this paper.